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LU Chao, JIAO Yangquan, PENG Yunbiao, WU Liqun, MIAO Aisheng, RONG Hui, XIE Huili. Paleo-interlayer oxidation zone identification and spatial localization prediction in Daying area[J]. GEOLOGY IN CHINA, 2018, 45(6): 1228-1240. DOI: 10.12029/gc20180612
Citation: LU Chao, JIAO Yangquan, PENG Yunbiao, WU Liqun, MIAO Aisheng, RONG Hui, XIE Huili. Paleo-interlayer oxidation zone identification and spatial localization prediction in Daying area[J]. GEOLOGY IN CHINA, 2018, 45(6): 1228-1240. DOI: 10.12029/gc20180612
shu

Paleo-interlayer oxidation zone identification and spatial localization prediction in Daying area

  • 1.

    China University of Geosciences, Wuhan 430074, Hubei, China

  • 2.

    No. 208 Geological Party, CNNC, Baotou 014010, Inner Mongolia, China

Funds: supported by National basic research program of China "973" Project, Sedimentary environment and large scale mineralization of continental basins in giant sandstone uranium metallogenic belt in North China (No. 2015CB453000), and threedimensional geological mapping of uranium bearing rocks on the northern margin of Ordos Basin project (No. 12120115013701)
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  • Author Bio:

    LU Chao, male, born in 1984, master candidate, engages in the study of uranium geology; E- mail: 56709507@qq.com

  • Received Date: October 30, 2016
  • Revised Date: January 24, 2017
  • Available Online: September 25, 2023
    Graphical Abstract
    • Abstract

  • Interlayer oxidation in potential uranium reservoir is closely related to uranium mineralization. Paleo-interlayer oxidation zone is considered to be an important symbol in search for sandstone type uranium deposits. In this paper, core drilling data and mineralogy and geochemical characteristics of each sub-band of interlayer oxidation were used to identify the paleo-interlayer oxidation. Combined with paleo-oxidic and reductive properties of uranium geochemical markers in uranium reservoirs, paleointerlayer oxidation was spatial positioned quantitatively. Accordingly, paleo-completely-oxidized zone and transitional zone and reduction zone were divided and identified. On such a basis, the distribution of paleo-interlayer oxidation zone controlled by the scale of the uranium reservoir, barrier layers, the dark mudstone and coal seam and other factors was discussed.

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    • References (63)
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